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(1887) Origin of Certain Banded Gneisses. Geological Magazine, S. 3 Vol. 4 (12) 573-574 doi:10.1017/s0016756800190697

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Reference TypeJournal (article/letter/editorial)
TitleOrigin of Certain Banded Gneisses
JournalGeological Magazine
Year1887 (December)Series:Volume3:4
Issue12
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800190697
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Mindat Ref. ID265371Long-form Identifiermindat:1:5:265371:0
GUID0
Full Reference(1887) Origin of Certain Banded Gneisses. Geological Magazine, S. 3 Vol. 4 (12) 573-574 doi:10.1017/s0016756800190697
Plain Text(1887) Origin of Certain Banded Gneisses. Geological Magazine, S. 3 Vol. 4 (12) 573-574 doi:10.1017/s0016756800190697
In(1887, December) Geological Magazine S. 3 Vol. 4 (12) Cambridge University Press (CUP)

See Also

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(1887) II.—On the Origin of certain Banded Gneisses. Geological Magazine, S. 3 Vol. 4 (11) 484-493 doi:10.1017/s0016756800190405
(1887) Rev. W. S. Symonds, M.A., F.G.S. Geological Magazine, S. 3 Vol. 4 (12) 574-576 doi:10.1017/s0016756800190703
(1876) International Geological Congress. Geological Magazine, S. 2 Vol. 3 (12) 573-574 doi:10.1017/s0016756800155815
(1890) Banded Rocks of the Lizard. Geological Magazine, S. 3 Vol. 7 (12) 574-575 doi:10.1017/s0016756800195883
(1902) ‘Sonorous’ Sand. Geological Magazine, S. 4 Vol. 9 (12) 573-574 doi:10.1017/s0016756800181609
(1892) Glacial Geology. Geological Magazine, S. 3 Vol. 9 (12) 573-574 doi:10.1017/s0016756800196311
(1895) Reports and Proceedings. Geological Magazine, S. 4 Vol. 2 (12) 573-574 doi:10.1017/s0016756800179051
(1903) Reports and Proceedings. Geological Magazine, S. 4 Vol. 10 (12) 573-574 doi:10.1017/s0016756800115444
(1887) Lydekker, Boulenger, and Dollo on Fossil Tortoises. Geological Magazine, S. 3 Vol. 4 (12) 572-573 doi:10.1017/s0016756800190685
(1899) Submerged Physical Features of the Mediterranean Basin. Geological Magazine, S. 4 Vol. 6 (12) 573-574 doi:10.1017/s001675680014292x
(1914) William Hill, V.P.G.S. Geological Magazine, S. 6 Vol. 1 (12) 573-574 doi:10.1017/s0016756800153646
 
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